Evidence of magma mixing identified in the Early Eocene Caina pluton from the Gangdese Batholith, southern Tibet
Abstract
Abundant mafic enclaves are enclosed within the Quxu batholith in the eastern Gangdese magmatic belt, southern Tibet. This study focuses on the petrogenesis and affinity of these mafic enclaves with their host diorite-granodiorite, as well as their mechanism of formation and tectonic setting. Zircon U-Pb geochronological and Hf isotopic results demonstrate that the mafic enclaves and their hosts were emplaced at ~ 50 Ma, with similar positive...
Paper Details
Title
Evidence of magma mixing identified in the Early Eocene Caina pluton from the Gangdese Batholith, southern Tibet
Published Date
May 1, 2017
Journal
Volume
278-281
Pages
126 - 139
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